Determining the growing season of land vegetation on the basis of plant phenology and satellite data in Northern China

被引:114
作者
Chen, XQ [1 ]
Tan, ZJ
Schwartz, MD
Xu, CX
机构
[1] Peking Univ, Dept Urban & Environm Sci, Beijing 100871, Peoples R China
[2] Peking Univ, Inst Remote Sensing & GIS, Beijing 100871, Peoples R China
[3] Univ Wisconsin, Dept Geog, Milwaukee, WI 53201 USA
基金
中国国家自然科学基金; 美国国家科学基金会;
关键词
growing season; plant phenology; NDVI; Northern China;
D O I
10.1007/s004840000056
中图分类号
Q6 [生物物理学];
学科分类号
071011 ;
摘要
The objectives of this study are to explore the relationships between plant phenology and satellite-sensor-derived measures of greenness, and to advance a new procedure for determining the growing season of land vegetation at the regional scale. Three phenological stations were selected as sample sites to represent different climatic zones and vegetation types in northern China. The mixed data set consists of occurrence dates of all observed phenophases for 50-70 kinds of trees and shrubs from 1983 to 1988. Using these data, we calculated the cumulative frequency of phenophases in every 5-day period (pentad) throughout each year, and also drew the cumulative frequency distribution curve for all station-years, in order to reveal the typical seasonal characteristics of these plant communities. The growing season was set as the time interval between 5% and 95% of the phenological cumulative frequency. Average lengths of the growing season varied between 188 days in the northern, to 259 days in the southern part of the research region. The beginning and end dates of the surface growing season were then applied each year as time thresholds, to determine the corresponding 10-day peak greenness values from normalized difference vegetation index curves for 8-km(2) pixels overlying the phenological stations. Our results show that, at the beginning of the growing season, the largest average greenness value occurs in the southern part, then in the northern, and finally the middle part of the research region. In contrast, at the end of the growing season, the largest average greenness value is measured in the northern part, next in the middle and lastly the southern part of the research region. In future studies, these derived NDVI thresholds can be applied to determine the growing season of similar plant communities at other sites, which lack surface phenological data.
引用
收藏
页码:97 / 101
页数:5
相关论文
共 21 条
[1]  
ACHARD F, 1990, PHOTOGRAMM ENG REM S, V56, P1359
[2]  
[Anonymous], AGR METEOROLOGY
[3]  
CHEN XQ, 1999, SCI GEOGRAPHICA SINI, V19, P21
[5]  
*I GEOGR CHIN AC S, 1989, CHIN YB AN PLANT PHE, V10
[6]  
*I GEOGR CHIN AC S, 1992, CHIN YB AN PLANT PHE, V11
[7]  
*I GEOGR CHIN AC S, 1989, CHIN YB AN PLANT PHE, V9
[8]   THE PATHFINDER AVHRR LAND DATA SET - AN IMPROVED COARSE RESOLUTION DATA SET FOR TERRESTRIAL MONITORING [J].
JAMES, ME ;
KALLURI, SNV .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1994, 15 (17) :3347-3363
[9]   MONITORING EAST-AFRICAN VEGETATION USING AVHRR DATA [J].
JUSTICE, CO ;
HOLBEN, BN ;
GWYNNE, MD .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1986, 7 (11) :1453-1474
[10]   ANALYSIS OF THE PHENOLOGY OF GLOBAL VEGETATION USING METEOROLOGICAL SATELLITE DATA [J].
JUSTICE, CO ;
TOWNSHEND, JRG ;
HOLBEN, BN ;
TUCKER, CJ .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1985, 6 (08) :1271-1318